Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Sergio, Rogledi"'
Autor:
Alessandro Maria Michetti, Francesca Giardina, Franz Livio, Karl Mueller, Leonello Serva, Giancanio Sileo, Eutizio Vittori, Roberto Devoti, Federica Riguzzi, Cipriano Carcano, Sergio Rogledi, Livio Bonadeo, Fabio Brunamonte, Gianfranco Fioraso
Publikováno v:
Annals of Geophysics, Vol 55, Iss 5 (2013)
It is commonly believed that the Po Plain is an area of low seismic hazard. This conclusion is essentially a combination of two factors: (1) the historical record of earthquakes, which shows a relatively small number of events of moderate magnitude,
Externí odkaz:
https://doaj.org/article/fed734ad4a694af0a4a67e74069876d4
Autor:
FABRIZIO TREMOLADA, ELISA GUASTI, GIANCARLO SCARDIA, CIPRIANO CARCANO, SERGIO ROGLEDI, DARIO SCIUNNACH
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 116, Iss 1 (2010)
Calcareous nannofossil and foraminiferal analyses have been carried out on outcrops from the type-area of the Gonfolite Lombarda Group (Como, northern Italy). In these marine fine- to coarse-grained clastics, rapidly accumulating at the southern fron
Externí odkaz:
https://doaj.org/article/71bf6fb082d84922bce0a84b36debba9
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 115, Iss 3 (2009)
This paper deals with the regional stratigraphy around the Alps-Apennines junction during late Eocene-Miocene. The basin-fill architecture and its relation to changes in structural style were deciphered through the integration of subsurface and outcr
Externí odkaz:
https://doaj.org/article/cf2e86e5edc54afc8f478e74895d0422
Publikováno v:
Marine and Petroleum Geology. 66:192-216
The Messinian reservoirs of Po Plain-Adriatic Basin were controlled by the combination of Messinian Salinity Crisis (MSC) and morphostructural reshaping. Under these conditions, complex sedimentary architectures and unusual stratigraphic discontinuit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2df890df8b350568d9563f03fa0b4437
https://doi.org/10.1016/j.marpetgeo.2014.12.012
https://doi.org/10.1016/j.marpetgeo.2014.12.012
Publikováno v:
Marine and Petroleum Geology. 42:50-81
During the Late Miocene–Pleistocene interval, a complex system of elongate foredeeps, the Po Plain-Adriatic Foredeep (PPAF), developed in the eastern sector of the Po Plain and in the northern Adriatic Sea, This system is the largest Late Miocene
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e8c6efc596a53f8e74a95d10b2f2f1d
https://doi.org/10.1016/j.marpetgeo.2012.11.007
https://doi.org/10.1016/j.marpetgeo.2012.11.007
Autor:
Manlio Ghielmi, Sergio Rogledi, Matteo Minervini, Massimo Rossi, Claudio Nini, Aimone Vignolo
Publikováno v:
RENDICONTI LINCEI. 21:131-166
In the last 15 years, several Eni-Agip multidisciplinary studies were focused on the buried Messinian–Pleistocene succession of the eastern Po Plain and northern Adriatic Sea. A detailed revision of the biostratigraphy, chronostratigraphy, sediment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::83532efed664dd80fa1eafdfcc1c996b
https://doi.org/10.1007/s12210-010-0101-5
https://doi.org/10.1007/s12210-010-0101-5
Publikováno v:
International journal of earth sciences (1999, Print) 99 (2010): 833–849. doi:10.1007/s00531-009-0428-2
info:cnr-pdr/source/autori:Mosca P.; Polino R.; Rogledi S.; Rossi M./titolo:New data for the kinematic interpretation of the Alps-Apennines junction (Northwestern Italy)./doi:10.1007%2Fs00531-009-0428-2/rivista:International journal of earth sciences (1999, Print)/anno:2010/pagina_da:833/pagina_a:849/intervallo_pagine:833–849/volume:99
info:cnr-pdr/source/autori:Mosca P.; Polino R.; Rogledi S.; Rossi M./titolo:New data for the kinematic interpretation of the Alps-Apennines junction (Northwestern Italy)./doi:10.1007%2Fs00531-009-0428-2/rivista:International journal of earth sciences (1999, Print)/anno:2010/pagina_da:833/pagina_a:849/intervallo_pagine:833–849/volume:99
Alps and Apennines are juxtaposed within an approximately 100 km-wide area covered by the Upper Eocene to Miocene successions of the Tertiary Piedmont Basin. The Upper Eocene-Oligocene evolution of this area was characterized to the north and west by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9184ea98c9b2d7bf7812efb62d8f023c
https://doi.org/10.1007/s00531-009-0428-2
https://doi.org/10.1007/s00531-009-0428-2
Publikováno v:
Geological Society of America Bulletin. 115:387-405
The integration of field and subsurface data permits a substantial revision of the sedimentary evolution of the Vena del Gesso basin, a thrust-top basin in the Northern Apennines where shallow-water primary gypsum deposits related to the Messinian sa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bf62f118c59e296a634e0ec3d62a9f70
https://doi.org/10.1130/0016-7606(2003)115<0387:sateot>2.0.co
https://doi.org/10.1130/0016-7606(2003)115<0387:sateot>2.0.co
Autor:
Andrea Argnani, G. Papani, Manlio Ghielmi, Luigi Torelli, Sergio Rogledi, Massimo Bernini, F. Rizzini, Giulia Barbacini, F. Camurri
Publikováno v:
Quaternary International. :13-26
The neotectonics of the Northern Apennines is illustrated using a crustal-scale geoseismic cross-section, based on seismic profiles and field mapping. The geological profile crosses a variety of tectonic settings, from the Val di Vara and Val Magra (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7898b140552dc690fdbceb1c896439af
https://doi.org/10.1016/s1040-6182(02)00088-5
https://doi.org/10.1016/s1040-6182(02)00088-5